Numerical Evaluation of the Modern and Future Origins of Atmospheric River Moisture Over the West Coast of the United States
Advanced Search
Select up to three search categories and corresponding keywords using the fields to the right. Refer to the Help section for more detailed instructions.

Search our Collections & Repository

For very narrow results

When looking for a specific result

Best used for discovery & interchangable words

Recommended to be used in conjunction with other fields

Dates

to

Document Data
Library
People
Clear All
Clear All

For additional assistance using the Custom Query please check out our Help Page

i

Numerical Evaluation of the Modern and Future Origins of Atmospheric River Moisture Over the West Coast of the United States

Filetype[PDF-7.44 MB]


Select the Download button to view the document
This document is over 5mb in size and cannot be previewed

Details:

  • Journal Title:
    Journal of Geophysical Research: Atmospheres
  • Personal Author:
  • NOAA Program & Office:
  • Description:
    Atmospheric rivers (ARs) are one of the major causes of extreme precipitation and flooding in many regions around the world and have been found to contribute substantially to global poleward moisture transport. However, the evaporative origin of the moisture in ARs remains unclear, at least on climatological timescales. Here we use the water tracer and water isotope‐enabled Community Atmosphere Model version 5 (CAM5) model to examine the moisture sources of ARs that impact the West Coast of the United States. The climatological distribution of moisture sources is determined for both the modern era and for 2100 under a Representative Concentration Pathway (RCP) 8.5 scenario. It is found that 33 to 53% of the precipitable water over the West Coast of the United States originates from the Northeast Pacific, in particular the midlatitudes and subtropics, although in June‐July‐August more moisture is recycled from continental regions. It is also found that although ARs are at least 70% Northeast Pacific moisture, a significant amount of the moisture is derived from tropical latitudes (>15% from south of 20°N). It is found that in the warmer 2100 climate there is a 39% increase in the magnitude of ARs. In this future epoch, moisture is transported from more remote regions for all seasons and for both ARs and the average climatology. To provide future observational evidence that this model result is robust, it is shown that water isotopes provide an observational constraint on the moisture transport pathways, and thus the possibility to observe changes in moisture source.
  • Keywords:
  • Source:
    JGR Atmospheres 123(12): 6423-6442, 2018
  • DOI:
  • Document Type:
  • Place as Subject:
  • Rights Information:
    Other
  • Compliance:
    Submitted
  • Main Document Checksum:
  • Download URL:
  • File Type:

Supporting Files

  • No Additional Files
More +

You May Also Like

Checkout today's featured content at repository.library.noaa.gov

Version 3.26.1